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    中国东部北黄海盆地东部坳陷岩浆活动特征及其与区域构造的耦合关系

    王任 石万忠 张先平 唐大卿 陈昊然 徐清海 徐壮

    王任, 石万忠, 张先平, 唐大卿, 陈昊然, 徐清海, 徐壮, 2017. 中国东部北黄海盆地东部坳陷岩浆活动特征及其与区域构造的耦合关系. 地球科学, 42(4): 587-600. doi: 10.3799/dqkx.2017.046
    引用本文: 王任, 石万忠, 张先平, 唐大卿, 陈昊然, 徐清海, 徐壮, 2017. 中国东部北黄海盆地东部坳陷岩浆活动特征及其与区域构造的耦合关系. 地球科学, 42(4): 587-600. doi: 10.3799/dqkx.2017.046
    Wang Ren, Shi Wanzhong, Zhang Xianping, Tang Daqing, Chen Haoran, Xu Qinghai, Xu Zhuang, 2017. Magmatic Activity Characteristics and Its Coupling Relationship with Regional Tectonics in the Eastern Depression of North Yellow Sea Basin, Eastern China. Earth Science, 42(4): 587-600. doi: 10.3799/dqkx.2017.046
    Citation: Wang Ren, Shi Wanzhong, Zhang Xianping, Tang Daqing, Chen Haoran, Xu Qinghai, Xu Zhuang, 2017. Magmatic Activity Characteristics and Its Coupling Relationship with Regional Tectonics in the Eastern Depression of North Yellow Sea Basin, Eastern China. Earth Science, 42(4): 587-600. doi: 10.3799/dqkx.2017.046

    中国东部北黄海盆地东部坳陷岩浆活动特征及其与区域构造的耦合关系

    doi: 10.3799/dqkx.2017.046
    基金项目: 

    国家十三五油气重大子课题 2016ZX05025002-003

    111引智项目 B14031

    国家基础地质调查项目 12120114055801

    详细信息
      作者简介:

      王任 (1990-),男,博士研究生,主要从事层序地层学、构造与沉积响应关系的研究工作.ORCID:0000-0002-6256-4683.E-mail: wangren1282@yahoo.com

      通讯作者:

      石万忠,ORCID:0000-0003-0207-708X.E-mail: shiwz@cug.edu.cn

    • 中图分类号: P548

    Magmatic Activity Characteristics and Its Coupling Relationship with Regional Tectonics in the Eastern Depression of North Yellow Sea Basin, Eastern China

    • 摘要: 如何深入了解中国东部北黄海盆地东部坳陷岩浆活动特征是目前研究的前沿之一.为探讨早白垩世异常剧烈岩浆活动的区域构造成因并揭示中国东部的构造动力学机制,利用井-震及岩浆岩测试资料,对北黄海盆地岩浆活动特征及其与区域构造的耦合关系进行研究.在空间上刻画了岩浆的侵入相、喷出相的地震反射特征及沿深大断裂展布的平面分布特征;在时间上划分出了包括早白垩世108~115 Ma、134~145 Ma在内的4期岩浆活动.结合区域地质分析认为早白垩世早期,伊泽奈琦板块沿北北西斜向俯冲于欧亚板块之下,太平洋板块向南西方向俯冲,板块剪切作用导致郯庐断裂带左旋走滑,使得盆地处于左旋伸展环境中,内部形成派生的北西向右旋、近南北向左旋的次级共轭断裂系并控制岩浆上侵底辟活动.经过综合分析,厘清了盆地岩浆活动及断裂演化过程与区域板块运动之间的耦合关系.

       

    • 图  1  北黄海盆地大地构造位置及构造分区

      a.据王嘹亮等 (2013)修改;b.底图为T5界面构造

      Fig.  1.  Tectonic location and divisions in North Yellow Sea basin

      图  2  北黄海盆地地层综合柱状

      龚承林等 (2009)修改

      Fig.  2.  Comprehensive stratigraphic column in North Yellow Sea basin

      图  3  北黄海盆地火山岩测井及岩性特征

      Fig.  3.  Logging and lithological characteristics of magmatic rocks in North Yellow Sea basin

      图  4  地震测线Line-1显示岩浆岩的喷出构造

      a.空白剖面;b.解释后的剖面;c.600 ms时间切片

      Fig.  4.  Ejected structure on seismic Line-1

      图  5  地震测线Line-2显示的岩浆岩侵入构造

      a.空白剖面;b.解释后的剖面;c.1 200 ms时间切片

      Fig.  5.  Intrusive structure on seismic Line-2

      图  6  研究区岩浆岩平面分布

      Fig.  6.  The distribution of magmatic rocks in the study area

      图  7  研究区断裂演化应力椭球体左旋剪切模式受力分析

      a.据王嘹亮等 (2013)修改;b.T5反射界面的断裂分布;①推测断裂;②朝鲜半岛西缘断裂;③郯庐断裂带;④南黄海北部断裂带

      Fig.  7.  The sinistral shear mode of fault evolution stress ellipsoid in study area

      图  8  研究区不同时期断裂分布

      a.T4界面断裂分布;b.T5界面断裂分布;c.T54界面断裂分布;d.Tg界面断裂分布

      Fig.  8.  Fault distribution map of different period in the study area

      图  9  研究区断裂演化应力椭球体右旋剪切模式受力分析

      a.据王嘹亮等 (2013)修改;b.T4反射界面的断裂分布;①.推测断裂;②.朝鲜半岛西缘断裂;③.郯庐断裂带;④.南黄海北部断裂带

      Fig.  9.  The dextral shear mode of fault evolution stress ellipsoid in study area

      图  10  早白垩世以来太平洋板块俯冲方向的演变

      Koppers (2001)修改

      Fig.  10.  The evolution of the Pacific plate subduction direction from Early Cretaceous to now

      图  11  燕山期中国东部周边依泽奈崎板块与太平洋板块位置复原

      Moore et al.(1990)修改

      Fig.  11.  The reconstructed location of Izanagi and Pacific plates during Yanshanian at eastern China

      图  12  岩浆活动及断裂演化过程与区域板块运动之间的耦合关系

      Fig.  12.  The coupling relationship between magmatic activity, fault evolution and regional plate movement

      表  1  研究区岩浆岩测年结果

      Table  1.   Test results of magmatic rocks in study area

      井名层段深度段 (m)厚度 (m)岩性年代 (Ma)
      Well-1J24 000.0~4 013.013.0玄武岩-
      Well-3J32 496.0~2 513.017.0花岗斑岩111.4±2.0
      Well-3J32 598.5~2 675.076.5英安岩141.0±2.0*
      Well-3J23 783.0~3 789.06.0英安岩145.0±2.0*
      Well-4J33 033.0~3 082.049.0花岗斑岩115.7±2.5
      Well-4J33 082.0~3 150.068.0花岗斑岩110.0±1.0
      Well-4J33 150.0~3 184.034.0花岗斑岩108.5±1.4
      Well-5J24 068.0~4 071.03.0辉绿岩-
      Well-5Pt4 390.0~4 430.040.0辉绿岩221.7±4.9
      Well-5Pt4 430.0~4 457.027.0辉绿岩238.1±3.5
      Well-5Pt4 457.0~4 478.021.0辉绿岩207.3±5.0
      Well-5Pt4 550.0~4 565.515.5辉绿岩-
      Well-6Pt3 566.0~3 576.010.0辉绿岩244.0
      Well-8J32 404.0~2 412.08.0花岗斑岩107.0±0.8
      Well-8J33 030.0~3 040.010.0花岗斑岩108.0±0.8
      Well-9J31 670.0~2 155.0485.0正长岩、闪长岩夹沉积岩-
      Well-10J32 447.0~2 993.0546.0粗面斑岩夹沉积岩-
      Well-10J33 162.0~3 330.0168.0安山岩、玄武质安山岩-
      注:*引用自王嘹亮等 (2015)
      下载: 导出CSV
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